| Institution | Faculty of Geosciences - Department of Earth and Environmental Science |
| Remuneration group | TV-L E13 |
| Full-time / Part-time | Part-time (75%) |
| Start date | 01.04.2026 or later (for three years) |
| Application deadline | 2026-01-31 |
In the research group for Sedimentology and Earth Surface Processes, we develop quantitative constraints on the physical and chemical processes that control the evolution of landscapes, the erosion, transport, and deposition of sediments, and the global fluxes of dissolved solutes and carbon. To this end, we combine field observations, analogue experiments, geochronological methods, and geochemical analyses of sediment, soil, and water. Part of the Faculty for Geosciences, the research group is embedded in an environment with a broad range of expertise from geology and geophysics to paleontology, mineralogy, and physical geography.
We are looking for you:
in Munich
Within the ERC-funded Project “Floodplain Weathering” (FloW), we are looking for a doctoral student that will use flume experiments and sediment samples to study controls on sediment transfer and storage on floodplains. The project is part of a larger effort to understand the impact of floodplain-sediment storage on the global carbon cycle. You will carry out large-scale flume experiments and laboratory work in Munich and at collaborating institutes in Utrecht. You will develop digital and analogue methods to track sediment and water and develop theory to interpret your findings. You will also communicate findings in peer-reviewed journals and during international conferences.
FloW
Rivers transport sediments from eroding uplands into sedimentary basins. Along this journey, sediments can be temporarily stored, building floodplains that support soil formation and development of weathering zones. Little is known about how fast sediments transition from mountains to lowlands, how many storage events they experience, and how the sediment residence time and storage depends on the grain size and on the climatic and tectonic boundary conditions. Beyond the relevance for fluvial geomorphology, this knowledge gap greatly limits our understanding of carbon cycling across floodplains. With FloW, we aim to develop a comprehensive understanding of the timescales of sediment transport and storage on floodplains and its impact on chemical weathering fluxes.
In this project within FloW, you will develop methods to trace sediment residence times across braided and meandering channel-belts in flume experiments. You will develop theory on the controls on sediment residence-time distributions. Together with fellow researchers working on FloW, you will test this theory against field data from the 1500-km-long floodplain of the Madeira River.
People with disabilities who are equally as qualified as other applicants will receive preferential treatment.
Inquiries prior to the application deadline can be directed to a.bufe@lmu.de.
To apply, please submit the following documents in English language, compiled into a single PDF file, to a.bufe@lmu.de by January 31th 2026:
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